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. 2016 May 9;7:666. doi: 10.3389/fmicb.2016.00666

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Copyright © 2016 Nawaz, Purahong, Lehmann, Herrmann, Küsel, Totsche, Buscot and Wubet.

This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

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Graphical illustration of groundwater wells in the Hainich Critical Zone Exploratory (Hainich CZE) at site H3 (located in grassland/pasture), H4 and H5 (located in agriculture/cropland) with their distances from the surface. The illustration is 4X vertically exaggerated. Groundwater samples were collected and analyzed from the sampling sites; H31, H41, and H51 (in Hainich transect lower – HTL aquifer assemblage) and H32, H43, H52, and H53 (in Hainich transect upper – HTU aquifers assemblage). Adapted base figure from Küsel et al. (2016).